Table 2.
R1013 |
R1014 |
|||||
---|---|---|---|---|---|---|
# | δσ (ppm) | ησ | δσ (ppm) | ησ | δσ (ppm)2 | ησ2 |
Cα | 26.3 | 0.48 | 24.6 | 0.51 | 26.0 | 0.36 |
Cβ | 10.3 | 1.0 | 10.8 | 1.0 | 11.0 | 1.0 |
C1 | 21.8 | 0.69 | 21.2 | 0.70 | … | … |
Cγ1 | 19.0 | 0.59 | 18.9 | 0.61 | 18.5 | 0.58 |
Cγ2 | 18.1 | 0.32 | 19.0 | 0.30 | 17.5 | 0.65 |
Co | 84.6 | 0.50 | 83.6 | 0.55 | 85.4 | 0.49 |
Note: R1013 and R1014 symmetry sequences were employed for σ2- and σ1-CSA recoupling. The MAS frequency was 10 kHz. Note that recoupling of 13C CSA is efficiently performed with these sequences for the natural abundance carbon sites in this sample.
Data reported for U-13C,15N-val enriched NAV sample (Reference 25).